
Magmatic Apatite: A Powerful, Yet Deceptive
... elongate). Equant apatite is generally defi ned by wellformed crystal faces (FIG. 1), and is often easily recognized by its hexagonal shape. This habit is interpreted to have grown under near-equilibrium conditions. Less commonly, equant apatite occurs with no well-formed crystal faces as an interst ...
... elongate). Equant apatite is generally defi ned by wellformed crystal faces (FIG. 1), and is often easily recognized by its hexagonal shape. This habit is interpreted to have grown under near-equilibrium conditions. Less commonly, equant apatite occurs with no well-formed crystal faces as an interst ...
Yin and yang of continental crust creation and destruction by plate
... when rates of ancient crust formation and destruction approximately agree with that of modern Earth support a hypothesis of formation by plate tectonic processes, whereas significant differences imply different processes, different rates, or both. As emphasized in the following sections, continental ...
... when rates of ancient crust formation and destruction approximately agree with that of modern Earth support a hypothesis of formation by plate tectonic processes, whereas significant differences imply different processes, different rates, or both. As emphasized in the following sections, continental ...
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... province. In (a): NAP, North America plate; PAP, Pacific plate; ERP, Eurasia plate; PSP, Philippine Sea plate; bold continuous line, plate boundary; fine continuous line with number (km), depth of subducting slab surface; dashed line, volcanic front; oval, volcanic chains and range; Μ, Quaternary vo ...
... province. In (a): NAP, North America plate; PAP, Pacific plate; ERP, Eurasia plate; PSP, Philippine Sea plate; bold continuous line, plate boundary; fine continuous line with number (km), depth of subducting slab surface; dashed line, volcanic front; oval, volcanic chains and range; Μ, Quaternary vo ...
Synthesis of Existing Structural Data for the Auckland Volcanic Field
... way down to the depths of magma generation (thought to be 80-100km beneath the surface in Auckland). Structures such as major crustal faults may provide easy pathways for ascending magma, and may ultimately control where the magma finally erupts. The better we understand the structural setting of th ...
... way down to the depths of magma generation (thought to be 80-100km beneath the surface in Auckland). Structures such as major crustal faults may provide easy pathways for ascending magma, and may ultimately control where the magma finally erupts. The better we understand the structural setting of th ...
The Influence of Lithospheric Flexure Induced by Volcano Loading
... The marine Erebus Basin surrounds the volcanic Ross Island in McMurdo Sound, Antarctica. This basin has evolved under the influence of flexure driven by loading by the three volcanoes that make up Ross Island. Seismic reflection data west of Ross Island are used to document the seismic stratigraphic ...
... The marine Erebus Basin surrounds the volcanic Ross Island in McMurdo Sound, Antarctica. This basin has evolved under the influence of flexure driven by loading by the three volcanoes that make up Ross Island. Seismic reflection data west of Ross Island are used to document the seismic stratigraphic ...
u series disequilibria: insights into mantle melting and
... rocks are both expected and usually observed to have (234U/238U) = 1, then 238U can essentially be treated as the parent of 230Th. It is important to remember that for all these U series nuclide pairs both the parent and daughter nuclides are unstable and will undergo radioactive decay at different ...
... rocks are both expected and usually observed to have (234U/238U) = 1, then 238U can essentially be treated as the parent of 230Th. It is important to remember that for all these U series nuclide pairs both the parent and daughter nuclides are unstable and will undergo radioactive decay at different ...
Adakitic Dacites Formed by Intracrustal Crystal Fractionation of
... pyroclastic eruption produced a fallout deposit composed of crystal-rich (30 vol.%, vesicle free) dacitic pumices (65^66 wt% SiO2) that are up to 40 cm in diameter in proximal areas, and that extend from the summit area to the SE for 20 km. The Lomas Limpias episode was characterized by the emplac ...
... pyroclastic eruption produced a fallout deposit composed of crystal-rich (30 vol.%, vesicle free) dacitic pumices (65^66 wt% SiO2) that are up to 40 cm in diameter in proximal areas, and that extend from the summit area to the SE for 20 km. The Lomas Limpias episode was characterized by the emplac ...
Hotspots and Melting anomalies - Earth and Environmental Sciences
... established the concept of “hotspot” as a broad swelling of topography capped by volcanism, which, combined with plate motion, generates volcanoes aligned in a chain and with ages that progress monotonically. In some cases, these chains project back to massive volcanic plateaus, or large igneous pro ...
... established the concept of “hotspot” as a broad swelling of topography capped by volcanism, which, combined with plate motion, generates volcanoes aligned in a chain and with ages that progress monotonically. In some cases, these chains project back to massive volcanic plateaus, or large igneous pro ...
Seamounts – characteristics, formation, mineral deposits and
... seamounts suggests that the Josephine Bank (north Atlantic) was perhaps the first identified seamount and in 1938, the term “seamount” was first officially given by the US Board of Geographic Names to the Davidson Seamount (Brewin et al., 2007). Until 1964, about 2000 seamounts had been discovered, ...
... seamounts suggests that the Josephine Bank (north Atlantic) was perhaps the first identified seamount and in 1938, the term “seamount” was first officially given by the US Board of Geographic Names to the Davidson Seamount (Brewin et al., 2007). Until 1964, about 2000 seamounts had been discovered, ...
Kurzlaukis and Lorenz_Gibeon Volcanic Field
... Signs of multiple intrusive activity within the kimberlite dikes have not been recognised. This is probably due to poor outcrop quality and the high degree of alteration of most of the kimberlites. The only exception is the carbonatitic dike near Mukorob, which shows vertical planar zonation. The in ...
... Signs of multiple intrusive activity within the kimberlite dikes have not been recognised. This is probably due to poor outcrop quality and the high degree of alteration of most of the kimberlites. The only exception is the carbonatitic dike near Mukorob, which shows vertical planar zonation. The in ...
1 MELT VISCOSITY, TEMPERATURE AND TRANSPORT
... Lower Pillow Lavas and the Basal Group. The divisions were based on mineralogy, color (alteration), and the abundance of dikes. An olivine phyric group at the top of the sequence constitutes the Upper Pillow Lavas resting on generally aphyric Lower Pillow Lavas. In the Upper Pillow Lava sequence, di ...
... Lower Pillow Lavas and the Basal Group. The divisions were based on mineralogy, color (alteration), and the abundance of dikes. An olivine phyric group at the top of the sequence constitutes the Upper Pillow Lavas resting on generally aphyric Lower Pillow Lavas. In the Upper Pillow Lava sequence, di ...
- ResearchOnline@JCU
... volcanic sequences form an aerially-extensive volcanic succession which is predominantly basaltic to andesitic and ranges in age from 54.8 to 35.4 Ma (Atherton et al., 1985; Noble et al., 1990; Section A). Oligocene mafic dykes also crop out throughout the region and have been recently dated at 29.4 ...
... volcanic sequences form an aerially-extensive volcanic succession which is predominantly basaltic to andesitic and ranges in age from 54.8 to 35.4 Ma (Atherton et al., 1985; Noble et al., 1990; Section A). Oligocene mafic dykes also crop out throughout the region and have been recently dated at 29.4 ...
Multi-Stage Origin of the Coast Range Ophiolite, Supra-Subduction Zone Ophiolites
... Jurassic sediments of the Great Valley Sequence. At other locales, plutonic rocks are scarce, the volcanic rocks are more like “oceanic” basalts (that is, basalts erupted at oceanic spreading centers or within oceanic plates), and contacts with sediments of the Great Valley Sequence may be faulted. ...
... Jurassic sediments of the Great Valley Sequence. At other locales, plutonic rocks are scarce, the volcanic rocks are more like “oceanic” basalts (that is, basalts erupted at oceanic spreading centers or within oceanic plates), and contacts with sediments of the Great Valley Sequence may be faulted. ...
Volcano

A volcano is a rupture on the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.Earth's volcanoes occur because its crust is broken into 17 major, rigid tectonic plates that float on a hotter, softer layer in its mantle. Therefore, on Earth, volcanoes are generally found where tectonic plates are diverging or converging. For example, a mid-oceanic ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates coming together. Volcanoes can also form where there is stretching and thinning of the crust's interior plates, e.g., in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande Rift in North America. This type of volcanism falls under the umbrella of ""plate hypothesis"" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so-called ""hotspots"", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Volcanoes are usually not created where two tectonic plates slide past one another.Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. One such hazard is that volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature; the melted particles then adhere to the turbine blades and alter their shape, disrupting the operation of the turbine. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere (or troposphere); however, they also absorb heat radiated up from the Earth, thereby warming the upper atmosphere (or stratosphere). Historically, so-called volcanic winters have caused catastrophic famines.